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논문 기본 정보

자료유형
학술저널
저자정보
Mehmet Aydin (강원대학교) Yeong-Sang Jung (강원대학교) Jae E. Yang (강원대학교) Hyun-Il Lee (강원대학교) Kyung-Dae Kim (강원도춘천농업기술원)
저널정보
한국토양비료학회 한국토양비료학회지 한국토양비료학회지 제45권 제4호
발행연도
2012.8
수록면
484 - 491 (8page)

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이 논문의 연구 히스토리 (2)

초록· 키워드

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The hydrological components of a sandy loam soil of nearly level in Chuncheon over 30 years were computed using the E-DiGOR model. Daily simulations were carried out for each year during the period of 1980 to 2009 using standard climate data. Reference evapotranspiration and potential soil evaporation based on Penman-Montheith model were higher during May to August because of the higher atmospheric evaporative demand. Actual soil evaporation was mainly found to be a function of the amount and timing of rainfall, and presumably soil wetness in addition to atmospheric demand. Drainage was affected by rainfall and increased with a higher amount of precipitation and soil water content. Excess drainage occurred throughout rainy months (from July to September), with a peak in July. Therefore, leaching may be a serious problem in the soils all through these months. The 30-year average annual reference evapotranspiration and potential soil evaporation were 951.5 ㎜ and 714.2 ㎜, respectively. The actual evaporation from bare soil varied between 396.9-528.4 ㎜ and showed comparatively lesser inter-annual variations than drainage. Annual drainage rates below 120 cm soil depth ranged from 477.8 to 1565.9 ㎜. The long-term mean annual drainage-loss was approximately two times higher than actual soil evaporation.

목차

Introduction
Materials and Methods
Results and Discussion
Conclusions
References

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UCI(KEPA) : I410-ECN-0101-2014-521-000807337